Tag: inversion

What is Delta T and why is it important for spraying?
Click here to listen to Audio Article
Humidity is important in spraying. With the average tank of pesticide being 90 to 99.5% water, evaporation plays an important role in both droplet size and active ingredient concentration. Low humidity causes droplets to evaporate faster, potentially increasing drift and reducing uptake. But relative humidity (RH) isn’t the best way to measure this effect because the same RH at two different temperatures results in two different water evaporation rates.
Instead, we present Delta T, also known as “wet bulb depression”. Delta T is an atmospheric moisture parameter whose use in spraying has made its way to North America from Australian operations. It is defined as the dry bulb temperature minus the wet bulb temperature, and provides a better indication of water evaporation rate than RH. Higher Delta T means faster water evaporation.
The recommendations from Australia are to avoid spraying when the Delta T is either too high or too low, with a range of two to eight being described as ideal.
Figure 1: Delta T chart used in Australia (Source: Australian Gov’t Dept of Meteorology)
Delta T is being reported on an increasing number of weather stations, and it’s time we took a closer look at what it means.
Measuring Relative Humidity
In the early days of weather reporting, relative humidity was calculated from psychrometric charts. All one needed was a hygrometer, usually a sling psychrometer. A sling psychrometer is two identical thermometers side by side whose bulbs could be slung in a circle, exposing them to moving air. One bulb was covered in a cotton wick moistened with distilled water, the other was left exposed and dry.
Figure 2: Sling psychrometer (Source: ScienceStruck.com)
As the bulbs met moving air, water evaporated from the cotton wick and that reduced the temperature of that thermometer. The dryer the air, the greater the evaporation rate and therefore the greater the temperature drop. The dry thermometer was unaffected by this movement.
On measuring the wet and dry bulb temperature, one consulted a psychrometric chart. This chart converted the two temperatures to total water content in the air, compared it to total water-holding capacity, and expressed it as Relative Humidity. Psychrometric charts are useful for many other air parameters such as dew point, vapour pressure, or enthalpy. (Pause briefly to give thanks that we don’t need to know what enthalpy is.)
Figure 3: Psychrometric Chart (Source: Carrier Corporation)
Turns out that RH is a poor measure of water evaporation rate. An RH of 24% at 20 C has exactly the same evaporation rate as an RH of 44% at 35 C. That’s why Delta T is the preferred measurement: it’s linearly related to evaporation.
Note: Modern electronic weather stations don’t need two thermometers to measure air moisture content, and use polymers whose capacitance or resistance changes with atmospheric moisture. Add an internal look-up table, and we have all the information we need.
Pros and Cons of Water Evaporation
It’s important to note that our Australian colleagues caution against spraying when water evaporation rate is both too high and too low.
Too High:
- Water evaporates rapidly, reducing droplet size and pre-disposing the smaller droplets to drift;
- Deposited droplets dry quickly, reducing pesticide uptake which is more effective from a wet deposit.
Too Low:
- Water doesn’t evaporate, maintaining the smaller droplets in a liquid state. These small droplets are already drift prone, but are now more potent because of more effective uptake. Overnight conditions that are inverted are usually humid, adding to harm potential from the inversion.
Delta T in North America
The addition of this parameter to our spraying weather lexicon has been useful. But it’s important to understand the context in which it was developed to properly judge its suitability.
Aussies started talking about Delta T because the use of finer sprays under the hot dry conditions found during their summer sprays resulted in significant evaporative losses, significantly greater drift potential, and potential reduction of product performance. The guidelines to avoid spraying when Delta T exceeds eight or ten originate there.
A few changes have happened since these guidelines were developed. Over the past ten to 20 years, we’ve observed greater use of low-drift sprays, with the coarser sprays’ larger droplets resisting fast evaporation. In the past five to ten years, water volumes have increased due to our heavier reliance on fungicides, desiccants, and contact modes of action. Both of these developments have helped reduce the impact of a dry atmosphere. We simply can’t say if a Delta T of 10 is too high with these new application methods.
Looking at it another way, if Delta T values are very high, increasing water volume and droplet size will mitigate that to some degree, as the Aussies state in their extension materials (linked earlier).
Formulation
Pesticide formulation can also play a role in evaporation. Once the water is gone, oily formulations may still have good uptake because the oily active ingredient stays dissolved in the oily solvents. This is both good and bad, helping on-target efficacy but also increasing the risk of more potent drift. Solutions, on the other hand, are more likely to leave their actives stranded on leaves as crystals once the water is gone.
Bottom Line
Delta T is definitely useful information when spraying. It will typically rise and fall with air temperature as the day proceeds, and it is wise to consider suspending operations when values are critical. Take note of the Delta T when spraying the same product throughout these hot days and learn from the experience. Remember, the atmosphere affects not just sprays but also plants and insects, and due to this complexity we may not be able to attribute success or failure to just one measurement.
June 19, 2018
Spray Drift – Why is it still happening?
Despite the abundance of information available on spray drift, we continue to see widespread incidents of damage to a variety of crops every year. Do applicators just not care or are they missing some vital information when making decisions to spray? I believe it is the latter.
What is the problem?
In my experience, the vast majority of spray drift cases (probably 90% or more) are the result of ‘inversion drift’. That means the drift has not come from an adjacent sprayed area, it has come from one or more sources that are some distance from the site of damage. The distance between the sprayed site and the location of the damage may vary dramatically, from a few kilometres to tens of kilometres.
Why is there so much inversion drift when labels specifically prohibit use of the products under surface temperature inversions? Many may argue that it is a blatant disregard of the label by a few applicators (translation = cowboy operators). I do not agree this is the main problem. While I can confirm the existence of ‘cowboy operators’, thankfully they are limited in number. I believe the problem is a lack of understanding about how to tell when there is an inversion and particularly not knowing how ‘day wind’ moves differently to ‘inversion wind’. I continue to see good farmers/applicators doing what they believe to be the right thing but it is not. These are people very concerned about minimizing spray drift; they honestly do not think they are doing anything wrong.
What is ‘day wind’?
After sunrise, the sun begins to heat the ground, the warm ground then heats the air close to the surface, and this air then rises. As that warm air rises, cold air from above sinks down to replace it. The ground then warms this cold air and it rises. This cycling of warm air rising and cold air sinking creates turbulence and then wind. This is a good thing; turbulent wind movement is much safer for spraying. ‘Day wind’ has a turbulent motion and is much more likely to pull any fine droplets to the ground within a reasonable distance. During the day, we can predict which direction and how far our fine droplets will travel.
What is ‘inversion wind’?
As the sun sets, the ground begins to cool quickly and this in turn cools the air next to the ground. As we all know, cold air does not rise and warm air does not sink. This means there is a layer of cold air trapped close to the surface and a layer of warm air above it. The result is no turbulent movement or mixing of the air. The air may become quite still and this is often observed around sunset when the daytime wind ceases or drops off. What happens next is where the real danger occurs for spraying.
As the night progresses and the ground cools more, the cool air close to the surface becomes colder and therefore more dense, particularly from midnight onwards. This cold dense air then begins to move across the landscape, often down slope and in very unpredictable directions. Remember this air is not turbulent, there is no mixing, it has layers of air, something like layers in plywood, and it flows parallel to the ground. Any fine droplets released into these layers of cold non-turbulent air will simply move sideways across the surface until the sun rises and heats the ground again. This is when the fine droplets are released from the layers and they come to ground, often in the lower parts of the catchment and a long way from the site of application. It is impossible to predict what direction this ‘inversion wind’ will go. For this reason, spraying in this type of wind is extremely high risk for spray drift.
Key indicators that and inversion is unlikely
- We should always expect that a surface temperature inversion has formed at sunset and will persist until sometime after sunrise unless we have one or more of the following: continuous overcast weather, with low and heavy cloud;
- continuous rain;
- wind speed remains consistently above 11km/h for the whole time between sunset and sunrise;
- and after a clear night, cumulus clouds begin to form.
Inversion wind movement – practical demonstration video
Wind is a key factor in any spray application. The problem is that not all wind is the same. To reduce the incidence of spray drift, it is critical that spray applicators understand how wind moves, particularly during a surface temperature inversion. This video uses smoke flares to visually demonstrate the air movement under inversion conditions.
Here’s what we’re looking for: moderate wind with consistent direction that disperses spray and drives it to ground.
Conclusion
Many factors affect the potential for spray to drift but the main ones are; the weather conditions at the time of application, nozzle selection, products/tank mix used, actual spray quality achieved, speed of rig, and boom height. The common denominator is that all of these things are within the control of the spray operator.
Spraying under inversion conditions is extremely high risk and prohibited on many product labels, that means it is illegal. If you are serious about preventing drift, then you must learn how to identify when an inversion is likely to be present and more importantly when it has broken.
All agricultural chemicals have the potential to drift; it is how we use them that increases or decreases that potential. Therefore, the problem is a human one, not a chemical one. There is a suite of information available but if you are still unsure or need any assistance, please seek advice from an expert. Maintaining long-term access to key products depends on us reducing spray drift.
March 8, 2017
Exploding Sprayer Myths (ep.5): Early Morning Spraying
Should you really get up before the birds to spray? There are a lot of good reasons for early morning and night spraying, but if you’re in a strong inversion, you might be in a world of hurt. Here’s episode 5 in our series of short, educational and irreverent videos made with Real Agriculture.
February 8, 2016
Debunking Sprayer Myths
Reproduced from an article written by Angela Lovell for Grainews, 2014
“The fundamental challenge of spraying is that it’s a compromise game,” said Tom Wolf of Agrimetrix Research and Training. “As operators and advisors we need to always balance the opposite needs of coverage, efficacy and drift.”
Wolf, in a presentation at the recent Manitoba Agronomists Conference in Winnipeg, sees a trend towards more fungicide use on farms across western Canada and technology that purports to make application more efficient. These trends include wider booms, faster speed capability, complex monitors, auto boom heights and bigger tanks.
As much as technology is a great thing, it’s still the operator that is the single most important part of any spray operation, so it’s important to make sure that he or she isn’t going out to the field with any conventional beliefs that simply aren’t correct.
The challenge with spraying is to control pests without harming you neighbour’s crops or the environment and over the years Tom Wolf has developed some pretty good ideas about how to do that and has had to dispel more than one popular myth about spraying.
Myth # 1: More pressure forces the spray into the canopy.
“There’s an element of truth to this but it’s forcing spray downward is the least thing that pressure does,” says Wolf. Spray pressure is primarily used to change spray flow rate. If you increase the pressure you will need to travel faster to allow the carrier volume to stay constant, and faster travel speed actually works against canopy penetration. Another important change is that spray quality will become finer with higher pressure. Finally, droplet velocity will initially increase, but even at higher pressure, small droplets still move slowly by the time they reach the canopy. “If you want to force a fine spray into the canopy, the best way to do that is to lower your boom, slow down, and increase the carrier volume,” says Wolf.
Myth # 2: Higher water volumes lead to run off.
There are two things that govern run off; droplet size and surface morphology of the leaf surface. “Anyone who says that anything more than 3 gallons/acre runs off the leaf surface is not telling you the whole picture,” says Wolf. “We’ve been unable to induce runoff from up to 200 US gpa in our tests, even using hard-to-wet grasses like green foxtail. Don’t be afraid of water. It’s a very good way of covering the canopies. Water gives you flexibility to use coarser sprays and that allows you to spray when it’s windier.”
Myth # 3: Spray drift is no issue for fungicides and insecticides
Aquatic organisms are extremely sensitive to most fungicides and insecticides. We might not see this effect, but it has a definite impact on our environment. It’s important to observe the buffer zones shown on product labels, which can vary depending on the product, the application method and the specific environment.
Myth # 4: Faster travel speeds save time and boost productivity
Wolf suggests evaluating this on a field by field basis. At faster speeds you lose control of the spray cloud and the finest droplets will go wherever the wind goes. Other problems with higher speeds are canopy penetration, pattern uniformity and pressure management. If you have an 800 gallon tank with an 80 ft boom and you are going 12 mph at 10 gallons/ac and your fill rate is 50 gallons per minute you are going to do about 84 acres/hour not including turns. If you go faster – 18 mph – you can do 110 acres/hour. But if you increase your fill speed, thereby decreasing the time spent filling you can increase productivity just as much. If you also increase your boom width you also increase productivity. “All I am asking is you don’t just look at travel speed to improve your productivity,” says Wolf.
Myth # 5: Double nozzles produce more droplets and improve coverage
“It’s the droplet size and water volume that drives the droplet numbers produced. It doesn’t matter how many nozzles produce this size,” says Wolf. Although some double nozzles produce finer droplets and therefore improve coverage, others actually produce coarse sprays which may decrease coverage. Pay attention to droplet size first – nozzle manufacturers publish spray qualities from their products. You can increase coverage from a single nozzle simply by increasing the spray pressure so yo produce a finer spray.
Myth # 6: Calm early mornings have the lowest drift risk
This is one of the biggest myths out there, says Wolf, and it’s all because of a condition called an inversion, which usually occur during clear nights, and which linger into the early morning hours. Under normal sunny daytime conditions, air currents rise, fall and disperse spray clouds rapidly but under inversion conditions they don’t. This can lead to severe drift issues, even significant distances away from the treated field.
Under sunny daytime conditions, air temperature cools with height and that allows for thermal turbulence to disperse the spray cloud. On clear nights, the temperature increases with height (the opposite temperature profile, therefore called an “inversion”), and this prevents air from mixing. As a result, the spray cloud will not disperse.
Assume that the atmosphere is inverted on clear summer nights, extending into a few hours after sunrise. Producers should never spray when an inversion is present, and a good indication might be if fog or smoke hangs in the air and not dispersing.
Myth # 7: A rate controller calibrates the sprayer
“Even with a $400,000 sprayer, the rate controller still relies on a single flow meter that sits at the back of the sprayer and measures the total flow to the boom. The operator has no idea where that total flow is going,” says Wolf. As a result, there is still no substitute for individual nozzle calibration. There are various new tools on the market to assist with that but they still need to be done individually.
Myth # 8: If I mess up agronomic decisions, I can correct that with a good spray application
A spray application has to be on time to be truly effective, says Wolf. In efficacy studies where yeield was measured, spraying herbicides “on time” (=early) produced a yield advantage over spraying just one week later, even with a spray quality that was so coarse that it resulted in relatively poor weed control. “If it’s breezy, use a low drift nozzle. This allows you the opportunity to spray on time,” he adds.
Myth # 9: Ammonia is a good general purpose tank cleaner
Ammonia raises pH and some chemicals like sulfonylurea products dissolve better at a higher pH. But if you have an oily emulsifiable concentrate (EC) formulation, either as a product or adjuvant, a soapy cleanout product will be needed. “Liberty exposes poor tank cleanout because the adjuvant in Liberty is such an excellent cleaner,” says Wolf. After use of an oily product, the use of a wetting agent such as AgSurf will assist in removing oily residue and many soap-based commercial cleaners are available.
Myth # 10: There is an optimal nozzle that does it all
“Right now a sprayer costs approximately 100,000 times more than the nozzle and the nozzle is still the part that makes you happy or sad,” says Wolf. “If we inverted the investment trend and said ‘let’s build a better atomizer’ there would be an optimal nozzle right now. But although we’ve made progress with low-drift nozzles recently, the industry still looks for inexpensive, simple ways to atmozie sprays.”
Spray quality is the language that is used when selecting nozzles. All manufacturers publish spray quality charts for their nozzles that also give recommended pressures to produce different spray qualities using a particular nozzle type. Spray qualities are colour coded and generally speaking the hotter (redder) the colour code the more drift-prone (finer) the spray. There are many nozzle choices and designs and typically grassy targets and contact products require nozzles that will produce Medium to Coarse spray quality. For broadleaf targets and systemic products a Coarse to Very Coarse spray quality can be used successfully. Selecting the right nozzle to produce the quality of spray required is important, says Wolf who recommends Coarse as a general purpose spray quality.
May 28, 2015